Difficulty: Easy
Correct Answer: Basalt
Explanation:
Introduction:
Construction materials often originate from different geological processes. Knowing whether a stone is volcanic (extrusive), plutonic (intrusive), or hypabyssal (shallow intrusive) helps predict texture, strength, durability, and typical uses in civil engineering.
Given Data / Assumptions:
Concept / Approach:
Igneous rocks are classified by where they solidify. Extrusive (volcanic) rocks cool quickly at the surface, producing fine-grained textures (e.g., basalt, rhyolite). Intrusive (plutonic) rocks cool slowly at depth, forming coarse-grained textures (e.g., granite). Hypabyssal rocks cool at shallow depths with intermediate texture (e.g., dolerite/diabase).
Step-by-Step Solution:
Verification / Alternative check:
Basalt forms from low-viscosity mafic lava flows, a hallmark of volcanic provinces (e.g., Deccan Traps). Granite, in contrast, crystallizes deep within the crust, giving large feldspar and quartz crystals; dolerite commonly occurs in dykes and sills with medium grains.
Why Other Options Are Wrong:
Granite: Intrusive, not extrusive; coarse grains indicate slow deep cooling.
Dolerite: Hypabyssal; neither deep intrusive nor extrusive; thus not volcanic in the strict sense.
All of the above: False because only basalt is volcanic.
Common Pitfalls:
Assuming any igneous rock is “volcanic.” The term volcanic specifically refers to extrusive rocks like basalt, pumice, and rhyolite.
Final Answer:
Basalt
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